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Geodesy is concerned with the measurement of position and movement of points on the earth’s surface. Its geophysical applications provide insights into many of the processes central to the earth and environmental sciences. Variations in the height of the ocean surface reflects variations in the earth’s gravity field caused by thermally driven motion in the solid mantle, the mechanism that is the basic driving mechanisms for the motion of the plates. Measurements of position and changes in position made with the Global Positioning System shows the patterns of deformation associated with the movement of the continents and mountain building, and help identify the forces causing them. A technique called interferometry that uses satellite radar observations can reveal what happens at depth on fault planes during earthquakes, what is the transient response of the earth following the earthquake, and how strain accumulates between earthquakes. Optical satellite images can also be used also to measure the surface displacements occurring in earthquakes, and to determine high-resolution topography that reveals the long-term effects of earthquake faulting.
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Tim Wright,John Elliott,Jin Fang, Andrew Hooper,Greg Houseman,Milan Lazecky,Yasser Maghsoudi, Qi Ou,Barry Parsons,Chris Rollins,Richard Styron,Hua Wang,
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